Plate Tectonics
... 2.) What is the evidence that supports continental drift? 3.) Why would you expect to see similar rocks and rock structures on two landmasses that were connected at one time? ...
... 2.) What is the evidence that supports continental drift? 3.) Why would you expect to see similar rocks and rock structures on two landmasses that were connected at one time? ...
File
... Earthquakes occur due to the sudden release of stored energy. This energy builds up over time due to the motion of crustal plates. When the energy is released, one plate suddenly moves relative to another—this causes seismic waves to travel through the surrounding rock. Primary waves, or P-waves, tr ...
... Earthquakes occur due to the sudden release of stored energy. This energy builds up over time due to the motion of crustal plates. When the energy is released, one plate suddenly moves relative to another—this causes seismic waves to travel through the surrounding rock. Primary waves, or P-waves, tr ...
chapter 8 ocean in the earth system
... ocean system? Viewed from space, the ocean is the most conspicuous component of the Earth system, covering 71% of the planet’s surface. For this reason, Earth is sometimes referred to as the water planet. The ocean consists of salt water occupying huge topographic depressions, the ocean basins. The ...
... ocean system? Viewed from space, the ocean is the most conspicuous component of the Earth system, covering 71% of the planet’s surface. For this reason, Earth is sometimes referred to as the water planet. The ocean consists of salt water occupying huge topographic depressions, the ocean basins. The ...
Chapter 2 Tectonic Theory (A)
... ◦ Earthquakes ◦ Faults ◦ Mountain belts ◦ Features of seafloor ...
... ◦ Earthquakes ◦ Faults ◦ Mountain belts ◦ Features of seafloor ...
Plate Boundaries
... O-O Convergent Boundary • When two oceanic plates collide, one runs over the other which causes it to sink into the mantle forming a subduction zone. • The subducting plate is bent downward to form a very deep depression in the ocean floor called a trench. • The worlds deepest parts of the ocean ar ...
... O-O Convergent Boundary • When two oceanic plates collide, one runs over the other which causes it to sink into the mantle forming a subduction zone. • The subducting plate is bent downward to form a very deep depression in the ocean floor called a trench. • The worlds deepest parts of the ocean ar ...
Plate Tectonics Test Review
... How does density of plates relate to plate tectonics and subduction? The plate that is more dense will go under (subduct) the other plate. ...
... How does density of plates relate to plate tectonics and subduction? The plate that is more dense will go under (subduct) the other plate. ...
Ch.4 Notes
... denser so subduction – goes under, continental crust goes up • Forms deep ocean trenches • Often forms volcanoes on land • 2. If continental crust plates are even both crumple and go up (Himalayas) • 3. oceanic and oceanic crusts one is subducted • Deep trench and island arc of volcanoes ...
... denser so subduction – goes under, continental crust goes up • Forms deep ocean trenches • Often forms volcanoes on land • 2. If continental crust plates are even both crumple and go up (Himalayas) • 3. oceanic and oceanic crusts one is subducted • Deep trench and island arc of volcanoes ...
File
... 1. What types of convergent boundaries will create volcanic activity? 2. Which type of boundary is know as the ...
... 1. What types of convergent boundaries will create volcanic activity? 2. Which type of boundary is know as the ...
pdf format
... During an earthquake, the ground shakes because of the release of elastic energy when the fault slips. How is this energy transmitted through rocks? ________________________. This effect is similar to energy passing across the surface of the ocean as water waves. It is only because rocks can behave ...
... During an earthquake, the ground shakes because of the release of elastic energy when the fault slips. How is this energy transmitted through rocks? ________________________. This effect is similar to energy passing across the surface of the ocean as water waves. It is only because rocks can behave ...
Word format
... The reason that faults fail abruptly when the friction is overcome is because the rocks build up a lot of energy by getting deformed before an earthquake. The rocks get pulled in opposite directions on either side of the fault, but they are locked together by the friction along the fault. What type ...
... The reason that faults fail abruptly when the friction is overcome is because the rocks build up a lot of energy by getting deformed before an earthquake. The rocks get pulled in opposite directions on either side of the fault, but they are locked together by the friction along the fault. What type ...
File - Mr. Tugman`s Earth Science
... As certain rocks form, they acquire the polarity that Earth’s magnetic field has at the time. These rocks possess paleomagnetism. How does a rock become magnetized? Many igneous rocks contain magnetite, an iron-rich mineral. As the rock cools and hardens, the iron-rich mineral grains become magnetize ...
... As certain rocks form, they acquire the polarity that Earth’s magnetic field has at the time. These rocks possess paleomagnetism. How does a rock become magnetized? Many igneous rocks contain magnetite, an iron-rich mineral. As the rock cools and hardens, the iron-rich mineral grains become magnetize ...
group 1 - WordPress.com
... Summary: Researchers have developed a model to simulate the impact of tsunamis generated by earthquakes and applied it to the Eastern Mediterranean. The results show how tsunami waves could hit and inundate coastal areas in southern Italy and Greece. A team of European researchers have developed a m ...
... Summary: Researchers have developed a model to simulate the impact of tsunamis generated by earthquakes and applied it to the Eastern Mediterranean. The results show how tsunami waves could hit and inundate coastal areas in southern Italy and Greece. A team of European researchers have developed a m ...
1-2 Notes: Continental Drift Continents Join Together and Split Apart
... South America and Western _____________________. There are many other fossils found around the world that support the theory of continental drift. Climate Greenland is an island near the Arctic circle that is covered in ice. BUT…Fossils of ____________________ plants can be found on the shores ...
... South America and Western _____________________. There are many other fossils found around the world that support the theory of continental drift. Climate Greenland is an island near the Arctic circle that is covered in ice. BUT…Fossils of ____________________ plants can be found on the shores ...
Why is the oldest ocean crust only ~180 Ma?
... What is the hydrotectonic cycle? What are the reservoirs of water in this cycle and how does water cycle between the reservoirs? ...
... What is the hydrotectonic cycle? What are the reservoirs of water in this cycle and how does water cycle between the reservoirs? ...
Plate Tectonics, and the Wilson Cycle
... What is the hydrotectonic cycle? What are the reservoirs of water in this cycle and how does water cycle between the reservoirs? ...
... What is the hydrotectonic cycle? What are the reservoirs of water in this cycle and how does water cycle between the reservoirs? ...
Lab 3&4 PowerPoint
... When comparing our model to the earth, what do the following parts of your model represent? • The heat source (candle): Core • The moving syrup: Mantle Convection • The cardboard pieces: pieces of the Earth’s crust ...
... When comparing our model to the earth, what do the following parts of your model represent? • The heat source (candle): Core • The moving syrup: Mantle Convection • The cardboard pieces: pieces of the Earth’s crust ...
Forces that Shape the Earth State Objectives 4.a.
... oceanic plate is forced below the less dense continental plate Oceanic plate melts as it pushes into the mantle forcing hot magma & gas up to the surface of the continent. Forms a deep-ocean trench & a long chain of continental ____________________. Ex. _________________ mountains of South Ame ...
... oceanic plate is forced below the less dense continental plate Oceanic plate melts as it pushes into the mantle forcing hot magma & gas up to the surface of the continent. Forms a deep-ocean trench & a long chain of continental ____________________. Ex. _________________ mountains of South Ame ...
Journey to the Center of the Earth Name: Stop 1 – Earth`s Surface
... Why is the lithosphere thinner under the oceans and thicker under the continents? ...
... Why is the lithosphere thinner under the oceans and thicker under the continents? ...
How The Earth Was Made: YELLOWSTONE
... 17. mountain ranges on the sea floor where divergent boundaries come apart 18. solid layer of the core 21. the plastic like layer of the mantle below the lithosphere 23. brittle layer of earth consisting of the crust and the upper portion of the mantle ...
... 17. mountain ranges on the sea floor where divergent boundaries come apart 18. solid layer of the core 21. the plastic like layer of the mantle below the lithosphere 23. brittle layer of earth consisting of the crust and the upper portion of the mantle ...
History of Deep Sea Biology - Monterey Bay Aquarium Research
... Reading for Sept. 29, Oct.1 Sept. 29 Physical Environment: • Gage and Tyler 1991. Chapter 2. Oct. 1 Faunal composition, depth zonation: • Carney, R.S. Zonation of deep biota on continental margins. 2005. Oceanogr. and Mar. Biol: An Annual Review 43: 211-278. • Gage and Tyler 1991. Skim through imag ...
... Reading for Sept. 29, Oct.1 Sept. 29 Physical Environment: • Gage and Tyler 1991. Chapter 2. Oct. 1 Faunal composition, depth zonation: • Carney, R.S. Zonation of deep biota on continental margins. 2005. Oceanogr. and Mar. Biol: An Annual Review 43: 211-278. • Gage and Tyler 1991. Skim through imag ...
Exploitation of sea-based resources and acidification
... Impacts of deep-sea mining include the creation of sediment plumes which affect marine life greatly. These plumes are caused by the residue from mining, once it is dumped back into the ocean. This creates a cloud of particles either on the surface of the water or on the seafloor. Near-bottom plumes ...
... Impacts of deep-sea mining include the creation of sediment plumes which affect marine life greatly. These plumes are caused by the residue from mining, once it is dumped back into the ocean. This creates a cloud of particles either on the surface of the water or on the seafloor. Near-bottom plumes ...
Seismic Waves - Fort Thomas Independent Schools
... core, but are refracted along the way, indicates that the inner core is denser than the outer core and solid. • When pressure dominates, atoms are squeezed together tightly and exist in the solid state. • If temperatures are high enough, atoms move apart enough to exist in the liquid state, even at ...
... core, but are refracted along the way, indicates that the inner core is denser than the outer core and solid. • When pressure dominates, atoms are squeezed together tightly and exist in the solid state. • If temperatures are high enough, atoms move apart enough to exist in the liquid state, even at ...
Why is the Ocean Salty?
... South Pacific, North and South Atlantic, Indian and Arctic Oceans and the Antarctic waters or seas. Scientists believe that the seas are as much as 500 million years old because animals that lived then occur as fossils in rocks which once were under ancient seas. There are several theories about the ...
... South Pacific, North and South Atlantic, Indian and Arctic Oceans and the Antarctic waters or seas. Scientists believe that the seas are as much as 500 million years old because animals that lived then occur as fossils in rocks which once were under ancient seas. There are several theories about the ...
Physical oceanography
Physical oceanography is the study of physical conditions and physical processes within the ocean, especially the motions and physical properties of ocean waters.Physical oceanography is one of several sub-domains into which oceanography is divided. Others include biological, chemical and geological oceanographies.